東華大學圖書館 |

Language: English

Help

回圖書館首頁

手機版館藏查詢

Back to Search results for [ null ]

Switch To: Labeled | MARC Mode | ISBD

Spatio-Temporal Patterns of Jet Stre...

Hudson, Amy R.

Linked to FindBook

Google Book

Amazon

博客來

Spatio-Temporal Patterns of Jet Stream Influence on Phenology.

Record Type:	Electronic resources : Monograph/item
Title/Author:	Spatio-Temporal Patterns of Jet Stream Influence on Phenology./
Author:	Hudson, Amy R.
Published:	Ann Arbor : ProQuest Dissertations & Theses, : 2020,
Description:	132 p.
Notes:	Source: Dissertations Abstracts International, Volume: 81-11, Section: B.
Contained By:	Dissertations Abstracts International81-11B.
Subject:	Natural resource management. -
Online resource:	http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=27741730
ISBN:	9798643172772

Spatio-Temporal Patterns of Jet Stream Influence on Phenology.
Hudson, Amy R.

Spatio-Temporal Patterns of Jet Stream Influence on Phenology. - Ann Arbor : ProQuest Dissertations & Theses, 2020 - 132 p.

Source: Dissertations Abstracts International, Volume: 81-11, Section: B.

Thesis (Ph.D.)--The University of Arizona, 2020.

This item must not be sold to any third party vendors.

Atmospheric circulation patterns are the primary mechanism by which energy is distributed in the midlatitudes across terrestrial ecosystems. Plant and animal phenology integrate the influence of seasonal atmospheric circulation patterns on surface weather events. As these drivers of climate variability change, and are projected to change, it is important to quantify the observed response of ecosystem growth and processes to drivers of climate variability across scales. In this dissertation, I merge phenology, climatology, and dendrochronology disciplines, novel data availability, and research computing, to quantify and visualize the influence of jet stream variability on phenology across scales: from the individual species to the hemisphere, and from seasons to centuries. First, I examined the influence of multiple seasonal atmospheric circulation indices on a network of trees growing in semi-arid conditions at high altitudes in the Bighorn Mountains, WY (Hudson et al. 2019, Dendrochronologia; Appendix A). While all 11 sites shared a majority of common variance- suggesting a common climate driver- I found that winter and spring circulation pattern signals in annual rings were possibly modulated by microclimate conditions dictating snowpack and water availability into the growing season. I then expanded from one region to the Northern Hemisphere and contracted to the satellite period to determine for which regional ecosystems the spring and fall Northern Hemisphere Jet stream (NHJ) Indices (Belmecheri et al., 2017 Earth Interactions) influenced the length of the growing season (Hudson et al., in prep; Appendix B). Spring and/or fall NHJ influenced length of season for 30% of our domain, although similar NHJ shifts in the spring and fall resulted in very different LOS response- possibly linked to the seasonal limiting factor of temperature and its modulation on water availability for specific land cover and climate types. The final portion of this dissertation focused on North America, where I examined the influence of monthly jet stream position on cross-continental monarch migration, as estimated by annual overwintering acreage in Mexico (Hudson et al., in prep; Appendix C). Remarkably, multiple months of jet stream position across the continent corresponded with monarch migration due to the influence on monarch physiology, flight conditions, and resource availability. Overall, spatio-temporal patterns of NHJ influence on growth varied by season and were very much system dependent. These patterns can be used for model benchmarking and to prioritize land management and conservation efforts in a warming world. A macrosystem ecology framework of phenology that includes seasonal atmospheric circulation patterns allows us to ultimately increase our predictive power of ecosystem response to a changing climate by 1) moving beyond trends in mean states to consider the variability and extreme events ecosystems are exposed to, and 2) emphasizing the connectivity of the landscape- particularly important for migrating organisms and when aggregating land surface response to climate change.

ISBN: 9798643172772Subjects--Topical Terms:

589570
Natural resource management.
Subjects--Index Terms:

Dendroclimatology

Spatio-Temporal Patterns of Jet Stream Influence on Phenology.
LDR:04318nmm a2200385 4500 001 2266270
005 20200608092722.5
008 220629s2020 ||||||||||||||||| ||eng d
020 $a 9798643172772
035 $a (MiAaPQ)AAI27741730
035 $a AAI27741730
040 $a MiAaPQ $c MiAaPQ
100 1 $a Hudson, Amy R. $3 3543457
245 1 0 $a Spatio-Temporal Patterns of Jet Stream Influence on Phenology.
260 1 $a Ann Arbor : $b ProQuest Dissertations & Theses, $c 2020
300 $a 132 p.
500 $a Source: Dissertations Abstracts International, Volume: 81-11, Section: B.
500 $a Advisor: Moore, David JP;Trouet, Valerie.
502 $a Thesis (Ph.D.)--The University of Arizona, 2020.
506 $a This item must not be sold to any third party vendors.
520 $a Atmospheric circulation patterns are the primary mechanism by which energy is distributed in the midlatitudes across terrestrial ecosystems. Plant and animal phenology integrate the influence of seasonal atmospheric circulation patterns on surface weather events. As these drivers of climate variability change, and are projected to change, it is important to quantify the observed response of ecosystem growth and processes to drivers of climate variability across scales. In this dissertation, I merge phenology, climatology, and dendrochronology disciplines, novel data availability, and research computing, to quantify and visualize the influence of jet stream variability on phenology across scales: from the individual species to the hemisphere, and from seasons to centuries. First, I examined the influence of multiple seasonal atmospheric circulation indices on a network of trees growing in semi-arid conditions at high altitudes in the Bighorn Mountains, WY (Hudson et al. 2019, Dendrochronologia; Appendix A). While all 11 sites shared a majority of common variance- suggesting a common climate driver- I found that winter and spring circulation pattern signals in annual rings were possibly modulated by microclimate conditions dictating snowpack and water availability into the growing season. I then expanded from one region to the Northern Hemisphere and contracted to the satellite period to determine for which regional ecosystems the spring and fall Northern Hemisphere Jet stream (NHJ) Indices (Belmecheri et al., 2017 Earth Interactions) influenced the length of the growing season (Hudson et al., in prep; Appendix B). Spring and/or fall NHJ influenced length of season for 30% of our domain, although similar NHJ shifts in the spring and fall resulted in very different LOS response- possibly linked to the seasonal limiting factor of temperature and its modulation on water availability for specific land cover and climate types. The final portion of this dissertation focused on North America, where I examined the influence of monthly jet stream position on cross-continental monarch migration, as estimated by annual overwintering acreage in Mexico (Hudson et al., in prep; Appendix C). Remarkably, multiple months of jet stream position across the continent corresponded with monarch migration due to the influence on monarch physiology, flight conditions, and resource availability. Overall, spatio-temporal patterns of NHJ influence on growth varied by season and were very much system dependent. These patterns can be used for model benchmarking and to prioritize land management and conservation efforts in a warming world. A macrosystem ecology framework of phenology that includes seasonal atmospheric circulation patterns allows us to ultimately increase our predictive power of ecosystem response to a changing climate by 1) moving beyond trends in mean states to consider the variability and extreme events ecosystems are exposed to, and 2) emphasizing the connectivity of the landscape- particularly important for migrating organisms and when aggregating land surface response to climate change.
590 $a School code: 0009.
650 4 $a Natural resource management. $3 589570
650 4 $a Climate change. $2 bicssc $3 2079509
650 4 $a Ecology. $3 516476
653 $a Dendroclimatology
653 $a Jet stream
653 $a Length of season
653 $a Macrosystem ecology
653 $a Migration
653 $a Phenology
690 $a 0528
690 $a 0404
690 $a 0329
710 2 $a The University of Arizona. $b Natural Resources. $3 1020934
773 0 $t Dissertations Abstracts International $g 81-11B.
790 $a 0009
791 $a Ph.D.
792 $a 2020
793 $a English
856 4 0 $u http://pqdd.sinica.edu.tw/twdaoapp/servlet/advanced?query=27741730